This core appears in the following publications:

Cofaigh, Colm {\'O} and Davies, Bethan J and Livingstone, Stephen J and Smith, James A and Johnson, Joanne S and Hocking, Emma P and Hodgson, Dominic A and Anderson, John B and Bentley, Michael J and Canals, Miquel and others
Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum
Quaternary Science Reviews, 2014
DOI: 10.1016/j.quascirev.2014.06.023
Cores in
this publication

Pudsey, Carol J and Evans, Jeffrey
First survey of Antarctic sub--ice shelf sediments reveals mid-Holocene ice shelf retreat
Geology, 2001
DOI: 10.1130/0091-7613(2001)029<0787:FSOASI>2.0.CO;2
Cores in
this publication

Core-related info:
Core name VC275
Setting marine
RegionPrince Gustav Channel, Eastern Antarctic Peninsula
Collection date 2000-03-11
IGSN ID
Core type vibrocore
Latitude -64.6017
Longitude -58.095
Water depth (m) 453.0
Core length (cm) 534.0
Comments

Cruise-related info:
CruiseJR48
Ship James Clark Ross
Cruise start date 2000-03-27
Cruise end date 2000-04-01

Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
772 0.0 - 0.0 Diatom-bearing clayey silt seasonal open-marine acid insoluble organic matter 6450.0 ± 40.0
776 47.0 - 47.0 Diatom-bearing clayey silt seasonal open-marine/sub-ice shelf distal from grounding line acid insoluble organic matter 11410.0 ± 40.0
777 84.0 - 84.0 Silty clay seasonal open-marine/sub-ice shelf distal from grounding line acid insoluble organic matter 14810.0 ± 50.0
773 107.0 - 107.0 Silty clay seasonal open-marine/sub-ice shelf distal from grounding line acid insoluble organic matter 18280.0 ± 60.0
774 124.0 - 124.0 Diamicton sub-ice shelf proximal to grounding line acid insoluble organic matter 22700.0 ± 70.0
775 176.0 - 176.0 Diamicton Subglacial acid insoluble organic matter 35470.0 ± 290.0

Depth-age relationship:
Plot key: black and gray bars represent 68.2% and 95.45% HPD interval(s), respectively.

Questions about this page: Ryan Venturelli